folds faults and other records of rock deformation ch 11 grotzinger jordan press siever
Download
Skip this Video
Download Presentation
Folds, Faults and Other Records of Rock Deformation Ch.11 Grotzinger, Jordan Press & Siever

Loading in 2 Seconds...

play fullscreen
1 / 45

Concepts you will need to know for the exams - PowerPoint PPT Presentation


  • 78 Views
  • Uploaded on

Folds, Faults and Other Records of Rock Deformation Ch.11 Grotzinger, Jordan Press & Siever . Concepts you will need to know for the exams. Deformation Normal fault Thrust/Reverse Fault Strike-slip Fault folds Stress tension   compression   shearing

loader
I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
capcha
Download Presentation

PowerPoint Slideshow about 'Concepts you will need to know for the exams' - huslu


An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.


- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript
concepts you will need to know for the exams
Concepts you will need to know for the exams
  • Deformation
  • Normal fault
  • Thrust/Reverse Fault
  • Strike-slip Fault
  • folds
  • Stress
  • tension 
  • compression 
  • shearing
  • Factors athat determine the amount and type of deformation in a rock
  • Temperature
  • Fluids
  • Pressure
  • How fast materials are deformed
  • Composition
  • Time
  • Fault breccia--- a example of brittle rock deformation
  • Mylonite ----- an example of plastic deformation
  • Joints fracturs and faults
  • Anticlines and Synclines
  • Dome, Valley and Ridge (TN) topography
slide3

A fold is a bend in a rock…

But, how can this be????

“Inequality is the cause of all local movements” LEONARDO DA VINCI (1452-1519)

slide5

A fault is a break in a rock across which there is observable movement.

When the break occurred an earthquake was generated, whether or not anyone was there to detect it.

Sometimes faults die at depth and do not break the surface. Sometimes they do such as for the Armenia 1988 earthquake.

slide8

Directed pressure (cf. confining) in the earth leads to deformation if it is great enough.

Rocks deform under three orientations for the directed pressure or STRESS.

slide9

The directed stress can have three orientations with respect to vertical:

(Side view)

(Side View)

(Bird’s Eye View)

slide10

If the sediments are “soft” and folds develop:

(Side view)

(Side View)

HIGHS

HIGHS

LOWS

LOWS

LOWS

(Bird’s Eye View)

slide14

If the sediments are brittle faults can develop:

(Side view)

(Side View)

(Bird’s Eye View)

slide15

If the sediments are brittle faults can develop:

(Side view)

(Side View)

(Bird’s Eye View)

slide17

What is the direction of directed pressure?

How many orientations of faults can be generated for the same directed pressure direction??

slide19

If the sediments two possible orientations for faults can develop:

(Side view)

(Side View)

(Bird’s Eye View)

slide20

At least 6 factors control how rock deforms

e.g. at shallow depth a rock may fracture whereas at depth it may flow.

Factors are:

(1) rock type

(2) Confining and directed pressure

(3) temperature

(4) Fluids

(5) Time

(6) Rate of deformation

slide21

Brittle: Means a rock breaks quickly into sharp pieces, e.g. glass at room temperature

Textures show that rocks break in a brittle fashion at shallow depths inside faults (I.e. fault breccia, fault flour)

slide23

Ductile-- Means that a rock breaks slowly,or has a lot of “give”

Textures show that rocks break in a ductile fashion at depths of a few kilometers inside faults. The minerals recrystallize, and grow into new shapes

slide25

Joints are also fractures, but which do not show clear movement of blocks across them.

( Remember: Faults are also fractures but WITH movement across the fractures)

slide27

Different types of faults imply different directions of shortening and lengthening and can be used to imply different types of plate margin settings:

ad